Abstract
The effect of spring snowmelt infiltration in a seasonal soil frost area on groundwater recharge was evaluated by systematically monitoring meteorological factors, soil temperature and humidity, groundwater table and temperature, electrical conductivity, and the value of δ18O in a small field site over a 2-year period. The variation of soil temperature and humidity, groundwater table during the freezing period, and the snowmelt period respectively, as well as their correspondence to the relevant environmental factors, and the influencing factors of the permeability of frozen layer were analyzed. The results showed that the evaluation of precipitation infiltration in seasonal soil frost areas should be divided into three stages: a non-freezing period, a freezing period, and a snowmelt period. Snow is the main form of precipitation during the freezing period, and groundwater cannot be recharged. During the snowmelt period of spring, the snow cover that accumulated during the freezing period infiltrates together with rainfall and has a significant effect on groundwater recharge. The general precipitation infiltration process occurs after the frozen soil thaws completely. These research results can improve the accuracy of groundwater recharge calculations for snowmelt infiltration in the seasonal soil frost area of Northeast China and provide a scientific basis for the evaluation and management of regional water resources.
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References
Appels, W. M., Coles, A. E., & Mcdonnell, J. J. (2018). Infiltration into frozen soil: from core‐scale dynamics to hillslope‐scale connectivity. Hydrological Processes, 32(1).
Barbecot, F., Guillon, S., Pili, E., et al. (2018). Using water stable isotopes in the unsaturated zone to quantify recharge in two contrasted infiltration regimes. Vadose Zone Journal, 17(1).
Bayard, D., Stähli, M., Parriaux, A., & Flühler, H. (2005). The influence of seasonally frozen soil on the snowmelt runoff at two Alpine sites in southern Switzerland. Journal of Hydrology, 309, 66–84.
Byun, K., Chiu, C. M., & Hamlet, A. F. (2019). Effects of 21st century climate change on seasonal flow regimes and hydrologic extremes over the Midwest and Great Lakes region of the US. Science of the Total Environment, 650, 1261–1277.
Cutforth, H., O’Brien, E. G., Tuchelt, J., & Rickwood, R. (2004). Long-term changes in the frost-free season on the Canadian prairies. Canadian Journal of Plant Science, 84, 1085–1091.
Fan, G. S., Zheng, X. Q., & Pan, G. Z. (1999). Experimental study on the influence of the buried depth of groundwater level on the infiltration characteristics of freeze-thaw soils. Journal of Hydraulic Engineering, 03, 21–26 (in Chinese).
Frauenfeld, O. W., Zhang, T., Barry, R. G., & Gilichinsky, D. (2004). Interdecadal changes in seasonal freeze and thaw depths in Russia. Journal of Geophysical Research: Atmospheres, 109.
Gao, Y., Hu, C. Y., Dong, Z., et al. (2000). A study on water movement trend during soil freezing. Scientia Silvae Sinicae, 04, 126–128 (in Chinese).
Gray, D. M., Brenda, T., Litong, Z., Pomeroy, J. W., & Granger, R. J. (2001). Estimating areal snowmelt infiltration into frozen soils. Hydrological Processes, 15, 3095–3111.
Hayashi, M., van der Kamp, G., & Schmidt, R. (2003). Focused infiltration of snowmelt water in partially frozen soil under small depressions. Journal of Hydrology, 270, 214–229.
Hirota, T., Pomeroy, J. W., Granger, R. J., & Maule, C. P. (2002). An extension of the force-restore method to estimating soil temperature at depth and evaluation for frozen soils under snow. Journal of Geophysical Research Atmospheres, 107, ACL-1-ACL 11-10.
Iwata, Y., Hayashi, M., & Hirota, T. (2008). Comparison of snowmelt infiltration under different soil-freezing conditions influenced by snow cover All rights reserved. Vadose Zone Journal, 7, 79–86.
Iwata, Y., Hayashi, M., Suzuki, S., Hirota, T., & Hasegawa, S. (2010). Effects of snow cover on soil freezing, water movement, and snowmelt infiltration: a paired plot experiment. Water Resources Research, 46, 2095–2170.
Jing, J. H., Han, S. P., Wang, X. Z., & Bai, M. (2007). The mechanism of water movement in the freezing-thawing process. Acta Geoscientica Sinica, 07, 50–54 (in Chinese).
Kane, D. L., & Stein, J. (1983). Water movement into seasonally frozen soils. Water Resources Research, 19, 1547–1557.
Lebeau, M., & Konrad, J. M. (2012). An extension of the capillary and thin film flow model for predicting the hydraulic conductivity of air-free frozen porous media. Water Resources Research, 48.
Li TX, Fu Q, Liu D (2009) Study on infiltration characteristic experiment of winter in cold areas. Research on water science and international rivers in cold region series 2. Study on water circulation and ice engineering in cold region — proceedings of “5th Conference on Water in Cold Region” (in Chinese).
Lin, L. (2008). Study on changes of rainfall infiltration recharge under conditions of variable environment in Songnen basin. Jilin university.
Niu, G. Y., & Yang, Z. L. (2006). Effects of frozen soil on snowmelt runoff and soil water storage at a continental scale. Journal of Hydrometeorology, 7, 937–952.
Pan, X., Helgason, W., Ireson, A., et al. (2017). Field-scale water balance closure in seasonally frozen conditions. Hydrology & Earth System Sciences Discussions, 21(11), 1–37.
Stähli, M., Jansson, P. E., & Lundin, L. C. (1996). Preferential water flow in a frozen soil – a two-domain model approach. Hydrological Processes, 10, 1305–1316.
Sutinen, R., Äikää, O., Piekkari, M., & Hänninen, P. (2009). Snowmelt infiltration through partially frozen soil in Finnish Lapland. Geophysica, 45, 27–39.
Suzuki, K., Kubota, J., Ohata, T., & Vuglinsky, V. (2006). Influence of snow ablation and frozen ground on spring runoff generation in the Mogot Experimental Watershed, southern mountainous taiga of eastern Siberia. Hydrology Research, 37, 21–29.
Watanabe, K., & Kugisaki, Y. (2017). Effect of macropores on soil freezing and thawing with infiltration. Hydrological Processes, 31(2), 270–278.
Zhang, H., Zhang, J. M., Zhang, Z. L., & Chai, M. T. (2016). Measurement of hydraulic conductivity of Qinghai-Tibet plateau silty clay under subfreezing temperatures. Chinese Journal of Geotechnical Engineering, 38(06), 1030–1035 (in Chinese).
Zhao, L., Gray, D. M., & Male, D. H. (1997). Numerical analysis of simultaneous heat and mass transfer during infiltration into frozen ground. Journal of Hydrology, 200, 345–363.
Zheng, X. Q., & Fan, G. S. (2000). Influence of moisture content on infiltration characteristics in seasonal frozen and thawed soil. Transactions of The Chinese Society of Agricultural Engineering, 06, 52–55 (in Chinese).
Zhou, Y. W., Guo, D. X., et al. (2000). Geocryology in China. Beijing: Science Press (in Chinese).
Funding
This work was funded by National Natural Science Foundation of China (41472213, 41602077, 41702252) and China Postdoctoral Science Foundation (149194).
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Du, X., Fang, M., Lv, H. et al. Effect of snowmelt infiltration on groundwater recharge in a seasonal soil frost area: a case study in Northeast China. Environ Monit Assess 191, 151 (2019). https://doi.org/10.1007/s10661-019-7285-7
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DOI: https://doi.org/10.1007/s10661-019-7285-7